Download presentation
Presentation is loading. Please wait.
1
By Team Funky Beams (+ Chuck)
The Ideal Array By Team Funky Beams (+ Chuck)
2
Preprocessing courtesy of Chuck
Download and unpack seed file Create and populate event directories with synchronized time windows of event sacs Remove instrument response Rotate ENZ to RTZ Preprocessing courtesy of Chuck
3
Select subset of OK array of interest
For the Z and T components For the gradiometer and the golay array For each array and frequency Determine array response For P and S waves Gradiometry analysis Compute Beamforming
4
Array Geometries and Co-Arrays
5
What is Beamforming? Rost & Thomas, 2002 5 stations array
Signals: time arrival (geometry,slowness) Plane wave Signals shifted with the phase slowness Stack Beamforming
6
Array Response Comparison (0.5-4 Hz)
Golay Grad H Cross
7
Array Response Comparison (1-12 Hz)
Golay Grad H Cross
8
Array Response Comparison (10-20 Hz)
Golay Grad H Cross
9
Earthquake within Fairview cluster
:29:38 (UTC) 98 km from OK array M 4.2
10
Beamforming - P wave Golay 0.51-25 Hz Golay 0.96-4.18 Hz
11
Beamforming - S wave Golay 0.51-25 Hz Golay 0.96-4.18 Hz
12
Beamforming Comparison
Hz Hz Hz Hz Hz P-wave S-wave
13
Line array
14
What is Gradiometry?
15
geometrical spreading
What is Gradiometry? geometrical spreading horizontal slowness
16
gradient of displacement
What is Gradiometry? gradient of displacement
17
numerically calculate numerically calculate
What is Gradiometry? numerically calculate numerically calculate measure invert
18
Gradiometry (Vertical) - Golay Array
Filtered Hz u(t) Azimuth Mean = Slowness Mean = Geo. Spr. Rad. Patt.
19
Gradiometry (Transverse) - Golay Array
Filtered Hz u(t) Azimuth Mean = 82.14 Slowness Mean = Geo. Spr. Rad. Patt.
20
Gradiometry (Vertical) - Gradiometer
Filtered 2-3 Hz u(t) Mean = Azimuth Slowness Mean = 0.165 Geo. Spr. Rad. Patt.
21
Gradiometry (Transverse) - Gradiometer
Filtered 2-3 Hz u(t) Mean = Azimuth Mean = Slowness Geo. Spr. Rad. Patt.
22
Thank you / merci beaucoup
Conclusions Aperture is an important control over the resolution Golay array is efficient for beamforming Station spacing heavily influences aliasing Gradiometry is more influenced by station spacing Thank you / merci beaucoup Chuck, IRIS, et al.!!!
23
Fin
Similar presentations
© 2024 SlidePlayer.com. Inc.
All rights reserved.